Carbonate minerals contain stable isotopes of carbon and oxygen with different masses
whose abundances and bond arrangement are governed by thermodynamics. The clumped …

Reconstructing the thermal history of minerals and fluids in continental environments is a
cornerstone of tectonics research. Paleotemperature constraints from carbonate clumped …

Stable carbon and oxygen isotopes (δ18O and δ13C values) and trace elements have been
applied to the study of diagenesis of carbonate rocks for over 50 years. As valuable as these …

Conventional carbonate–water oxygen isotope thermometry and the more recently
developed clumped isotope thermometer have been widely used for the reconstruction of …

Many fields of Earth sciences benefit from the knowledge of mineral formation temperatures.
For example, carbonates are extensively used for reconstruction of the Earth's past climatic …

Septarian carbonate concretions contain carbonate precipitated during progressive growth
of the concretion and subsequent fracture-filling. As such, they have been used to track …

We utilize carbonate clumped isotope thermometry to explore the diagenetic and thermal
histories of exhumed brachiopods, crinoids, cements, and host rock in the Permian …

Rationale Mass‐47 CO2 clumped isotope thermometry requires relatively large (~ 20 mg)
samples of carbonate minerals due to detection limits and shot noise in gas source isotope …

Subsurface characterization of faults and fault systems is a central piece to describe the
subsurface permeability architecture of a carbonate reservoir during field development. Data …

In this study, we analyze the fault and fracture network of the Middle Triassic carbonate
platform of the Lastoni di Formin (Italian Dolomites, Italy). The reconstruction of the …